Appreciation: paleobotany!

Discussion in 'Maples' started by emery, Apr 19, 2014.

  1. emery

    emery Renowned Contributor Maple Society 10 Years

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    My wife gave me a very cool birthday present, a maple fossil. It's a lovely thing for a maple fan, if you're looking for a present for one, you can't go wrong with this one. :)

    Here is Acer tricuspidatus. From Brezanky in Czech, miocene period (23 - 5.3 million years old). Amazing!

    -E
     

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  2. JT1

    JT1 Contributor 10 Years

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    Amazingly priceless! Happy birthday!
     
  3. emery

    emery Renowned Contributor Maple Society 10 Years

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    Thanks John!
     
  4. AlainK

    AlainK Renowned Contributor Forums Moderator Maple Society 10 Years

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    Lucky you! ;-)

    Do you have any info or links to Acer tricuspidatus? I can't find much on this species with a search engine, any hints on to what it evolved, or where it can be found if it's still alive somewhere?...
     
  5. emery

    emery Renowned Contributor Maple Society 10 Years

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    I don't know much about it, or not yet anyway. ;) MOW mentions briefly that A. tricuspidatum Braun (1845) is in section Rubra and was found most frequently in the Upper Oligocene to Middle Miocene, 40-16 MYBP (million years before present). I wonder if there are fossil pollen and flowers around which make it possible to classify that precisely. There is also an interesting graph on p. 66 (of my edition) showing evolution of the basil portion of the leaf in A. tricuspidatum during the "Middle European Tertiary", which puts mine late Miocene.

    To my eye it looks a lot like A. monspessulanum, but clearly that's not meaningful... :) I'm pretty sure it's extinct though!

    This paper http://bomax.botany.pl/pubs/data/article_pdf?id=77 has some information, and gives the attribution to Bronn (not Braun as in MOW). It states that the contemporary relative is A. rubrum.
     
    Last edited: Apr 20, 2014
  6. AlainK

    AlainK Renowned Contributor Forums Moderator Maple Society 10 Years

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    Thanks a lot, Emery.
     

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